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Global shallow sediment diagenesis survey results based on all available IODP...
Global shallow sediment diagenesis survey results based on all available IODP sediment core images. -
(Table 4) Composition of turbidite and background samples at ODP Site 166-1007
Sediment depth is given as mbsf. The first Miocene sample was picked at a depth of 311.65 mbsf. -
(Table 3) Composition of turbidite and background samples at ODP Site 166-1003
Sediment depth is given as mbsf. The first Miocene sample was picked at a depth of 331.3 mbsf. -
(Table 1) Range table of planktonic foraminifers from ODP Hole 166-1006A sedi...
This dataset has no description
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(Appendix) Bathyal benthic foraminifera in ODP Hole 166-1006A sediments
The percent carrying capacity Kp is the equilibrium population in percentage terms of a species that an area can support while adequately meeting the needs of every individual.... -
(Table 1) Benthic foraminifer stratigraphy of ODP Site 166-1006 sediments
Site 1006 provides a middle to late Miocene record of bathyal benthic foraminiferal abundance changes in the Straits of Florida. Benthic foraminifers indicate that sedimentation... -
(Table 3) Uranium and thorium concentrations, ratios and ages of sediments fr...
Sediment depth is given in mcd. Raw age is calculated directly from the data in the previous two columns. Scavenging corrected age = the age corrected for initial 230Th by... -
(Table 1) Th and U isotope ratios of sediments from ODP Site 166-1009
U and Th blanks are <1‰ of the measured sample and are corrected for. Raw ages and delta234U values are adjusted to account for initial 230Th to give the corrected numbers in... -
(Table 1) Th and U isotope ratios of sediments from ODP Site 166-1008
U and Th blanks are <1‰ of the measured sample and are corrected for. Raw ages and delta234U values are adjusted to account for initial 230Th to give the corrected numbers in... -
(Table 1) TIMS U and Th concentrations and isotope ratios of ODP Leg 166 sites
AGE is the corrected age -
U and Th concentrations and U-TH ages for bulk carbonate samples from ODP Hol...
Thirty-one new bulk-sediment U–Th dates are presented, together with an improved d18O stratigraphy, for ODP Site 1008A on the slopes of the Bahamas Banks. These ages supplement... -
(Table 1) Age determination of ODP Leg 166 holes
Thick, late Quaternary sediment sections were recovered at several sites on the leeward slope of Great Bahama Bank during Leg 166 of the Ocean Drilling Program. These sections... -
Chemical and Sr isotopic compositions of 3 step leachates and residues of bul...
Massive clinoptilolite authigenesis was observed at about 1105 meters below sea floor (mbsf) in lower Miocene wellcompacted carbonate periplatform sediments from the Great... -
U and Th concentrations and isotope ratios of samples from ODP Leg 166
Constraining the history of seawater (234U/238U) is important because this ratio is used to assess the validity of U/Th ages, and because it provides information about the past... -
U-Th dating of marine sediments from the Bahamas slope
In order to understand the driving forces for Pleistocene climate change more fully we need to compare the timing of climate events with their possible forcing. In contrast to... -
Uranium concentrations and isotope ratios Bahamas seawater and ODP holes pore...
The geometry, timing, and rate of fluid-flow through carbonate margins and platforms is not well constrained. In this study, we use U concentrations and isotope ratios measured... -
Depths and ages of seismic sequence boundaries in ODP Leg 166 holes
High-resolution, multichannel seismic data collected across the Great Bahama Bank margin and the adjacent Straits of Florida indicate that the deposition of Neogene-Quaternary... -
Composition of hardgrounds and of pore-water parameters in ODP Holes 166-1008...
Mineralogic, petrographic, and geochemical analyses of sediments recovered from two Leg 166 Ocean Drilling Program cores on the western slope of Great Bahama Bank (308 m and 437... -
Stable isotope, seismic sequence boundaries and bioevents in ODP Hole 166-1006A
During ODP Leg 166, the recovery of cores from a transect of drill sites across the Bahamas margin from marginal to deep basin environments was an essential requirement for the... -
Sediment composition and sedimentation rates of four Holes in ODP Leg 166
To date, work on the Great Bahama Bank's western, leeward margin has centred chiefly on seismic-scale expressions of carbonate sequences and systems tracts. However,...
